1. Estuaries and Deltas
Estuary = semi-enclosed coastal environment where freshwater and ocean water meet and mix
Delta = sedimentary deposit at mouth of river that causes coastline to protrude into ocean
Reading Material
“The Estuarine Environment”, from “The World Ocean”
W.A. Anikouchine and R.W. Sternberg, Prentice-Hall
“River Deltas”, from “The Coast of Puget Sound”
J.P. Downing, Puget Sound Books
“River Deltas”, from “Coasts”
R.A. Davis, Prentice-Hall

2. Impact of sea-level rise on fluvial and glacial valleys
20,000 y to 7,000 y ago
valleys flooded, all sediment trapped
7,000 y ago to present
if little sediment supply – estuaries and fjords still filling
trapping mechanisms very important
(Chesapeake Bay)
if moderate sediment supply – estuaries nearly full
some sediment leaks to continental shelf
(Columbia River)
if much sediment supply – estuaries full and sediment overflowing
deltas build seaward
(Mississippi Delta)

3. Chesapeake and Delaware Bays
Coastal-Plain Estuaries
Drowned river valleys

4. Impact of sea-level rise on fluvial and glacial valleys
20,000 y to 7,000 y ago
valleys flooded, all sediment trapped
7,000 y ago to present
if little sediment supply – estuaries and fjords still filling
trapping mechanisms very important
(Chesapeake Bay)
if moderate sediment supply – estuaries nearly full
some sediment leaks to continental shelf
(Columbia River)
if much sediment supply – estuaries full and sediment overflowing
deltas build seaward
(Mississippi Delta)

5. Some sediment from Columbia River escapes estuary and accumulates on the adjacent continental shelf.
Prevailing transport mechanisms carry sediment northward, and most accumulates on the middle shelf

6. Impact of sea-level rise on fluvial and glacial valleys
20,000 y to 7,000 y ago
valleys flooded, all sediment trapped
7,000 y ago to present
if little sediment supply – estuaries and fjords still filling
trapping mechanisms very important
(Chesapeake Bay)
if moderate sediment supply – estuaries nearly full
some sediment leaks to continental shelf
(Columbia River)
if much sediment supply – estuaries full and sediment overflowing
deltas build seaward
(Mississippi Delta)

7. Active portion of Mississippi Delta
The shape is a bird-foot delta
Flooded river valley (estuary) filled, and sediment is (was) building coastline seaward

8. Types of Estuaries Estuary = semi-enclosed coastal environment where freshwater and ocean water meet and mix
Coastal-Plain estuary (drowned river valley)
V shape in cross section – result of fluvial erosion
horn shape (i.e., triangular) in map view – water floods to topographic contour lines
example: Chesapeake Bay
Fjord (drowned glacial valley)
U shape in cross section, deep – result of glacial erosion
shallow sill at mouth
examples: high latitudes, Alaska, Scotland, Scandinavia, Chile

9. Types of Estuaries

10. Types of Estuaries Bar-built estuary (lagoon)
sand spit or barrier island encloses embayment
shallow
example: Willapa Bay
Tectonic estuary
down-dropped basin (due to plate tectonics)
located near ocean, and seawater floods basin example: San Francisco Bay (not very common)

11. Estuarine Sedimentation
relevant to rivers – end of fluvial processes
relevant to beaches – traps or releases sediment to beach
Sand supplied by rivers (10%)
transported as bedload (and suspended load)
trapped near head of estuary
where gradient of river surface goes to zero (sea level)
Mud supplied by rivers (90%)
transported as suspended load
trapped throughout estuary
critical processes: water circulation
particle flocculation

12. Distinction between particle transport as bedload and suspended load
Note that “saltation” is intermediate between bedload and suspended load

13. Sediment Transport Bedload gravel = >2 mm
sand = 2 mm to mm (or 64 microns)
particles bounce and roll along bottom
relatively slow means of transport
erosion depends on particle size
Suspended load
silt = mm to mm (64-4 microns)
clay = <0.004 mm (<4 microns)
particles float with water
relatively fast means of transport
erosion depends on particle size and degree of consolidation

14. Erosion curve for different grain sizes
Velocity necessary to erode gravel and sand depends on grain size
Velocity necessary to erode silt and clay depends on size, but also the degree of consolidation
Consolidation = how much water has been removed from between particles

15. Estuarine Circulation
Salt wedge

16. Estuarine Circulation
Salt wedge
fresh water at surface moving seaward
boundary with underlying salt water = halocline
friction with salt water, causes mixing
some salt water carried seaward with fresh water
new salt water moves landward, near bottom
therefore, landward bottom current = salt wedge
Fjord circulation
shallow sill inhibits exchange of deep water
oxygen is consumed by animals in deep water behind sill
anoxia (absence of oxygen) can develop, and animals die

17. Fjord Circulation Deep sill thorough mixing of deep water Shallow sill
poor mixing of deep water

18. Particle Flocculation
Flocculation = formation of aggregates from individual silt and clay particles
Electrical charges at surface (due to breaks in mineral structure)
mostly negative charges
fresh water - particles repel each other
brackish/salt water – particles attracted to each other
form flocs
Flocs are larger than particles and sink faster
Silt and clay particles have platey shape
particles join end to face, forming “card-house” structure
sediment reaches bed of estuary with much water within flocs
(ultimately leads to consolidation of delta surfaces)

19. Floc Characteristics
Individual silt and clay particles are platey in shape
Flocs are formed with “cardhouse” structure
Water separates particles
Bed deposit initially has much space filled with water

20. Turbidity Maximum Turbidity = sediment in suspension
Fluvial suspended particles carried seaward in surface water
they flocculate and sink
Estuarine suspended particles carried landward in bottom water
They meet at the halocline and cause highest turbidity in estuary
this is the turbidity maximum
Base of turbidity maximum is where most particles deposit on bed
Location of turbidity maximum moves upstream and downstream:
over hours, due to tides
over months, due to seasonal changes in river discharge
Ultimately, muddy sediment deposits over most of estuary
ESTUARIES ARE EXCELLENT SEDIMENT TRAPS

21. Estuarine Circulation

22. River Deltas Evolve from coastal-plain estuaries
Rivers with much sediment filled their estuaries during the past ~7000 y
sea-level rise was slow
estuaries are excellent sediment traps
Infilled estuaries have triangular shape = Greek letter Δ
from shape of Nile Delta
Sediment supply must be able to overcome:
slow rise in sea level
tectonic subsidence
erosion by tides, waves, currents
consolidation of sediment accumulating

23. Nile Delta Flowing northward into Mediterranean Sea
Two primary distributaries today
Waves rework shoreline into cuspate shape

24. Global Distribution of Deltas

25. Location and Shape of Deltas
Deltas found many places in world
most common where river with much sediment enters protected setting
e.g.: small body of water (Mediterranean Sea, Gulf of Mexico, Puget Sound)
behind island or reef (Trinidad, Great Barrier Reef)
behind seasonal sea ice (Bering Sea, Arctic Ocean)
Where river reaches sea level, it divides into smaller distributary channels
Shape of protrusion from shoreline depends on oceanographic processes
weak waves and tidal currents: each distributary channel builds seaward
“bird-foot” delta builds with delicate digitation
strong waves: longshore drift smears sediment along coast
cuspate shape forms
strong tidal currents: distributary channels eroded and expanded
islands formed between broad channels

26. Active portion of Mississippi Delta
The shape is a bird-foot delta
Sedimentation is associated with individual distributary channels
These form because tidal currents are very weak and waves are generally very small

27. Sao Francisco Delta
Waves rework shoreline into cuspate shape

28. Fly River Delta
Classic example of tide-dominated delta – tidal currents enlarge distributary channels

29. Classification
of deltas

30. Location and Shape of Deltas
Deltas found many places in world
most common where river with much sediment enters protected setting
e.g.: small body of water (Mediterranean Sea, Gulf of Mexico, Puget Sound)
behind island or reef (Trinidad, Great Barrier Reef)
behind seasonal sea ice (Bering Sea, Arctic Ocean)
Where river reaches sea level, it divides into smaller distributary channels
Shape of protrusion from shoreline depends on oceanographic processes
weak waves and tidal currents: each distributary channel builds seaward
“bird-foot” delta builds with delicate digitation
strong waves: longshore drift smears sediment along coast
cuspate shape forms
strong tidal currents: distributary channels eroded and expanded
islands formed between broad channels

32. Deltaic Sedimentation
Ocean

33. Deltaic Sedimentation
Estuarine processes (e.g., flocculation, turbidity max) displaced into ocean
Topset (uppermost region)
freshwater swamps, brackish water marshes, sandy channel floors
sediment accumulation controlled by sea-level rise
land surface sinks due to consolidation of underlying mud
Foreset (middle region)
very high rates of sediment accumulation = thick, muddy deposits
sloped surface (few degrees)
gullies form from turbidity currents, landslides occur from slope failure
Bottomset (deepest region)
forerunner of advancing delta
thin deposits of mud over inner-shelf sand
Lobe of maximum sedimentation changes over centuries
depression filled, and lobe switches to another location

34. Fraser River Delta

35. Main Channel
Smaller Slope Gullies
Submarine Channel System

36. slide or creep

37. Deltaic Sedimentation
Estuarine processes (e.g., flocculation, turbidity max) displaced into ocean
Topset (uppermost region)
freshwater swamps, brackish water marshes, sandy channel floors
sediment accumulation controlled by sea-level rise
land surface sinks due to consolidation of underlying mud
Foreset (middle region)
very high rates of sediment accumulation = thick, muddy deposits
sloped surface (few degrees)
gullies form from turbidity currents, landslides occur from slope failure
Bottomset (deepest region)
forerunner of advancing delta
thin deposits of mud over inner-shelf sand
Lobe of maximum sedimentation changes over centuries
depression filled, and lobe switches to another location

38. History of lobe switching for the Mississippi Delta
The Mississippi Delta has switched its lobe of active sedimentation many times during the past several thousand years
The active lobe of the Mississippi is the Balize

39. Active portion of Mississippi Delta
The shape is a bird-foot delta
Sedimentation is associated with individual distributary channels
These form because tidal currents are very weak and waves are generally very small